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- W2264412797 abstract "The discovery in 1950 of this 75-million bbl complex of oil pools was based largely on the belief that a large stratigraphic Dakota oil pool would be found updip from a well in which permeable oil-saturated Dakota sandstone was found to be water-bearing. The Dakota oil reservoir is a complex of interlocking sandstone bodies deposited in a shallow sea. Although Dakota oil reserves basically are trapped updip by a permeability barrier, a spectacular tilt of 750 ft (230 m) in the oil-water contact along the south side of the pool argues, in part, for a dynamic balance between water flow and the oil accumulation. The lower Muddy pool occurs in point-bar sandstones from a filled stream channel which meandered across a well-defined meander belt. Only 2 positions of the stream channel are evident; therefore, the meander belt is only partially filled. The third set of stratigraphic oil pools within the South Glenrock oil field is found in 4 marine bar sandstones which were deposited after marine burial of the earlier Muddy stream channels and associated topography." @default.
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- W2264412797 date "1972-01-01" @default.
- W2264412797 modified "2023-09-27" @default.
- W2264412797 title "South Glenrock Oil Field, Wyoming: Prediscovery Thinking and Postdiscovery Description" @default.
- W2264412797 doi "https://doi.org/10.1306/m16371c29" @default.
- W2264412797 hasPublicationYear "1972" @default.
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